A transient ice sheet model simulation of the past 3 million years suggests that the Antarctic Ice Sheet became more sensitive to decreasing CO2 levels following the Mid-Pleistocene Transition, driven by the increasing influence of global sea-level changes…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
- Palaeoclimate constraints narrow uncertainty in future Arctic winter sea ice projections
- Progressive oxidative weathering raised sub-arc mantle fugacity on the Archaean Earth
- An abrupt shift towards a hotter and drier climate regime in the Western Eurasian Steppe
- Dry pebble rain could have delivered water to Earth through hydrogen reduction of iron oxide
- Rethinking Agulhas Leakage impacts on Atlantic circulation
- Atmospheric lessons from Mars
- Ice clouds born from Martian waves
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